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Mantle Materials
Mantle Materials

... Upper Mantle Olivine • Olivine – Thought to be about 10-12% Fe in upper mantle • At pressures around the 410-km discontinuity, Fo-rich olivine transforms to a ccp structure called wadsleyite. • Iron rich olivines do not undergo this transformation. At higher pressures, both the Fa-rich olivine and ...
File
File

... 11. What are fossils? 12. List at least 3 ways they are formed or found 13. Draw a diagram showing how the fossils of a bird would be found if they were 10 years old, 25 years old, and 50 years old 14. What does the term geological history refer to? 15. What makes a petrified fossil special? 16. Do ...
- Maheshtala College
- Maheshtala College

... The Earth is composed of four different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball sm ...
Earthquake Vocabulary - Garnet Valley School District
Earthquake Vocabulary - Garnet Valley School District

... moves the ground up and down or side to side ...
Tectonic Terror
Tectonic Terror

... deposit minerals at different locations. Thanks to volcanic activity, tin, silver, gold, copper and even diamonds can be found in volcanic rocks. Most of the metallic minerals mined around the world, particularly copper, gold, silver, lead and zinc are associated with rocks found below extinct volca ...
Ch.2 Tectonics
Ch.2 Tectonics

study
study

... 28 Which of the following are the three major types of rocks? ...
Plate Tectonics and the Ocean Floor opens with a brief history of
Plate Tectonics and the Ocean Floor opens with a brief history of

... reversals in polarity of Earth’s magnetic field 4. Radiometric age dating establishes that ocean floor is youngest at mid-ocean ridge and oldest toward continents ...
Plate: a rigid slab of solid lithosphere rock that has defined
Plate: a rigid slab of solid lithosphere rock that has defined

... a rigid slab of solid lithosphere rock that has defined boundaries and floats on the denser rocks of the asthenosphere a point on the earth’s surface where strong upward convection currents or plumes of hot magma in the upper mantle push up below the plates of the lithosphere causing volcanic ...
Folded Mountains
Folded Mountains

... By Patti Hutchison ...
Earth as a System
Earth as a System

...  Inner core: ________________iron and __________________& sulfur ...
Sedimentary rock
Sedimentary rock

... • How does the differences on where rock form effect the type of texture it has? • Explain both compaction and cementation: ...
V.V. Beloussov (1907-1990) Famous opponent of plate tectonics
V.V. Beloussov (1907-1990) Famous opponent of plate tectonics

... Marine magnetic anomalies are not uniform and thickness not proportional to anomaly age (but he doesn’t know about magnetic “skewness” due to interaction with earth’s field) ...
Sea-Floor Spreading
Sea-Floor Spreading

Unit 2 Earth Structures 1. The movement of tectonic plates is so slow
Unit 2 Earth Structures 1. The movement of tectonic plates is so slow

... B. Earthquakes take place where energy is transferred to rock by the motion of tectonic plates. C. Earthquakes can only occur at places where magma can reach the surface and transfer energy to rocks. D. Earthquakes take place when one plate moves over another plate, which happens only at plate bound ...
Review Questions, Chapter 7, 12th Ed.
Review Questions, Chapter 7, 12th Ed.

... 7. Both are dip-slip movements in which one block moves up and the other down along the fault surface. Assume that dip-slip faults with vertical dips (the fault surface is vertical) are normal faults. For dipslip faults with inclinations or dips other than vertical, the hanging wall–footwall designa ...
Layers of the Earth
Layers of the Earth

... • Fossils tell us the kinds of different organisms that inhabited (lived in) specific environments during ...
Structure of the Earth powerpoint
Structure of the Earth powerpoint

... • Earth was formed roughly 4.6 billion ears ago and for a long time was entirely molten. • The various materials (elements) that make up the earth were stratified (separated) according to their density. • The densest elements formed the core and the lighter elements floated to the surface. ...
Plate Tectonics Bingo - Western Reserve Public Media
Plate Tectonics Bingo - Western Reserve Public Media

... Plates: The earth’s surface is broken into seven large and many small moving plates, each about 50 miles thick. They move relative to one another an average of a few inches a year or about as fast as fingernails grow. Plate Tectonics: The term for the field of study of large scale motions of the ear ...
Lecture 7 Review Sheet
Lecture 7 Review Sheet

... What is the difference between a mineral being of BIOGENIC origin and being INORGANIC? What is the difference between a natural mineral and a synthetic mineral? What is the difference between a mineral simulant and a real mineral? What are two primary ways by which minerals form on Earth? What is th ...
Notes # ______ Sea Floor Spreading Mid Ocean Ridge underwater
Notes # ______ Sea Floor Spreading Mid Ocean Ridge underwater

... shaped like ​ pillows​  or ​ squeezed­out toothpaste​  in the central valley of mid­ocean ridges.  These rock formations only form when ​ magma erupts underwater and hardens very quickly​ ...
Unit 10: Layers of the Earth
Unit 10: Layers of the Earth

Unit F Chapter 1 Test
Unit F Chapter 1 Test

... Conduction Convection ...
Chapter 4 Plate tectonics Review Game
Chapter 4 Plate tectonics Review Game

... core, outer core ...
hawaii_vaolcanos
hawaii_vaolcanos

... http://www.unexplained-mysteries.com/forum/index.php?showtopic=157659 When molten lava chills quickly, a thin, glassy rind forms on the exposed surfaces because crystallization of the minerals in the melt could not take place in such a short time. This layer of glass provides the iridescent luster t ...
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Geochemistry

Geochemistry is the science that uses the tools and principles of chemistry to explain the mechanisms behind major geological systems such as the Earth's crust and its oceans. The realm of geochemistry extends beyond the Earth, encompassing the entire Solar System and has made important contributions to the understanding of a number of processes including mantle convection, the formation of planets and the origins of granite and basalt.
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